{"id":86601,"date":"2018-03-10T00:11:12","date_gmt":"2018-03-10T00:11:12","guid":{"rendered":"https:\/\/www.deberes.net\/tesis\/sin-categoria\/caracterizacion-de-las-precipitaciones-intensas-a-escala-diaria-en-el-pais-valenciano\/"},"modified":"2018-03-10T00:11:12","modified_gmt":"2018-03-10T00:11:12","slug":"caracterizacion-de-las-precipitaciones-intensas-a-escala-diaria-en-el-pais-valenciano","status":"publish","type":"post","link":"https:\/\/www.deberes.net\/tesis\/geografia\/caracterizacion-de-las-precipitaciones-intensas-a-escala-diaria-en-el-pais-valenciano\/","title":{"rendered":"Caracterizacion de las precipitaciones intensas a escala diaria en el pais Valenciano."},"content":{"rendered":"<h2>Tesis doctoral de <strong> Rafael Armengot Serrano <\/strong><\/h2>\n<p>Se analizan las precipitaciones superiores a 100mm en el d\u00eda pluviom\u00e9trico en el pa\u00eds Valenciano y su entorno inmediato en el periodo 1976-90, desde una triple perspectiva:  &#8211; caracterizaci\u00f3n pluviom\u00e9trica.- Se estudia su distribuci\u00f3n espacial estacional e interanual y su aportaci\u00f3n volum\u00e9trica. Se establecen correlaciones entre datos m\u00e1ximos, \u00e1reas afectadas y vol\u00famenes precipitados, y se define un \u00edndice de focalizaci\u00f3n. As\u00edmismo se estudian los centros de masa y se clasifican estad\u00edsticamente los 130 d\u00edas intensos en conglomerados.  &#8211; caracterizaci\u00f3n sin\u00f3ptica. Se define el contexto favorable a la lluvia intensa en funci\u00f3n de la presencia de baja aislada en 500 hpa, y se efect\u00faa un estudio de los 575 d\u00edas que en el per\u00edodo cumplen dicha condici\u00f3n. Se analiza el car\u00e1cter reforzante e inhibidor de toda una serie de variables sin\u00f3pticas en los distintos niveles troposf\u00e9rivos. Se estudia en detalle la advecci\u00f3n en capas y el gradiente en superficie, y se efect\u00faa una climatolog\u00eda de las bajas en 500 hpa y su eficiencia pluviom\u00e9trica.  &#8211; modelizaci\u00f3n estad\u00edstica. Se han efectuado modelos de regresi\u00f3n log\u00edstica para predecir la ocurrencia de lluvia intensa desde una doble perspectiva: precipitaci\u00f3n m\u00e1xima puntual y altos vol\u00famenes totalizados. Se aborda mediante componentes principales y mediante variables independientes y de s\u00edntesis. se comprueba el aceptable comportamiento de los modelos mediantevalidaci\u00f3n cruzada, y se propone un sistema de alerta para la predicci\u00f3n de lluvias intensas en tiempo real.<\/p>\n<p>&nbsp;<\/p>\n<h3>Datos acad\u00e9micos de la tesis doctoral \u00ab<strong>Caracterizacion de las precipitaciones intensas a escala diaria en el pais Valenciano.<\/strong>\u00ab<\/h3>\n<ul>\n<li><strong>T\u00edtulo de la tesis:<\/strong>\u00a0 Caracterizacion de las precipitaciones intensas a escala diaria en el pais Valenciano. <\/li>\n<li><strong>Autor:<\/strong>\u00a0 Rafael Armengot Serrano <\/li>\n<li><strong>Universidad:<\/strong>\u00a0 Universitat de val\u00e9ncia (estudi general)<\/li>\n<li><strong>Fecha de lectura de la tesis:<\/strong>\u00a0 27\/09\/2000<\/li>\n<\/ul>\n<p>&nbsp;<\/p>\n<h3>Direcci\u00f3n y tribunal<\/h3>\n<ul>\n<li><strong>Director de la tesis<\/strong>\n<ul>\n<li>Alejandro Perez Cueva<\/li>\n<\/ul>\n<\/li>\n<li><strong>Tribunal<\/strong>\n<ul>\n<li>Presidente del tribunal: joan francesc Mateu belles <\/li>\n<li>Javier Martin vide (vocal)<\/li>\n<li>sergio Alonso oroza (vocal)<\/li>\n<li>Jorge Tamayo carmona (vocal)<\/li>\n<\/ul>\n<\/li>\n<\/ul>\n<p>&nbsp;<\/p>\n","protected":false},"excerpt":{"rendered":"<p>Tesis doctoral de Rafael Armengot Serrano Se analizan las precipitaciones superiores a 100mm en el d\u00eda pluviom\u00e9trico en el pa\u00eds [&hellip;]<\/p>\n","protected":false},"author":1,"featured_media":0,"comment_status":"open","ping_status":"open","sticky":false,"template":"","format":"standard","meta":{"site-sidebar-layout":"default","site-content-layout":"","ast-site-content-layout":"","site-content-style":"default","site-sidebar-style":"default","ast-global-header-display":"","ast-banner-title-visibility":"","ast-main-header-display":"","ast-hfb-above-header-display":"","ast-hfb-below-header-display":"","ast-hfb-mobile-header-display":"","site-post-title":"","ast-breadcrumbs-content":"","ast-featured-img":"","footer-sml-layout":"","theme-transparent-header-meta":"","adv-header-id-meta":"","stick-header-meta":"","header-above-stick-meta":"","header-main-stick-meta":"","header-below-stick-meta":"","astra-migrate-meta-layouts":"default","ast-page-background-enabled":"default","ast-page-background-meta":{"desktop":{"background-color":"var(--ast-global-color-4)","background-image":"","background-repeat":"repeat","background-position":"center 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